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Polyphase deformation of mylonites from the Renco gold mine (Zimbabwe): identified by crystallographic preferred orientation of quartz.<I> Journal of Structural Geology</I>, 25, 253-262.51

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Polyphase deformation of mylonites from the Renco gold mine (Zimbabwe): identified by crystallographic preferred orientation of quartz.<I> Journal of Structural Geology</I>, 25, 253-262.5030020

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